Meteorological Statistics. xxiii 
TABLE IV.—Bzarzy—Interior of Canterbury, at 2104 feet above the sea. 
1877. 
Mean Extreme Range Mean Mean Mean 
Mean j|dailyrange| range Barometer of Elastic |Degree of Total lAmount 
Annual of of EN ng | Barome-| Force of | Moisture Rainfall. of 
Temp. | Temp. for | Temp. for ter for |Vapour for (o Cloud 
year. year. ed year. year. year. 1 
Degrees.| Degrees. | Degrees. Inches. Inches. | Inches. | Sat.=100.| Inches. | 0 to 10 
46-0 15:8 71:0 29:715* 1:434 :205 65 106:414 5:0 
* Reduced to sea level. 
TABLE V.—EARTHQUAKES reported in New Zzarawp during 1877. 
s E TE 
PLACE E S |. I g 5 E als 
8|. a) 8 |e E B 2 Ao]|»rels 
ea D £g a B D o o Q e 
HIRATA IS in] h |a o O JZJIAJS 
Taranaki vectes ee d IRL. x à i a 1 
Napier PS a (idi s scbescl ae d 2 
Taupo ve bac uu clNLI. es : 8*1 2 
Manawatu e BF cts Sere, IE Um Zu "a Em T 
Wanganui ot PE PIA D IT IAÓ š A 2 
Wairoa ala cda dulasd. 1. BENI 1 
Foxton es [ok eid E e s * E. 1 
Wellington | |10* 9,10 4,16 | 11 | 122" 10 |o, 7| ^ | 12 
$ : UR : j 59 š 
Blenheim x. sur. iE $ oe ae sge 
Picton.. Etc d S aS i è F 22* . L 
Havelock Se re ee Ses weirs 2. 22* lul a 
n LU OQ qon a JU ALS EHE a a : 2 
UEM = 1.1. 1.51. .] 4* d fae toe aoe et 
byielton. —.1..413 |. cbe Tubo ; ae : 
aia nob tar tertre ae Ge vi 16 coda 
i ee ee LE ee ee . LI ees ee 9* . 
p cd eT anl ulus R i s : TIL 
acsi sch ds Salene oue v* . 9* P : 
Queen: te owes T : š s TH i x. 9 
Upper $ Shotove [sos eae 18*| 1. es Se RA š 
urgh tn ERE ; ludi is eee 
ER tha Ug cron e x ee aie )* 
Palmerston Sth. i 2: ; oe = Es 5 PL d. 
Oam L4 ee *- oe LJ *. . 1 . . 
Naseby . ee . oe oe LE . LI . 9* ee 1 
Timaru es PPG We sos T Ta A l.l. 1 
Wi i te se > ee os oe fr LE oo. LE LI 0 .. oe 1 
Kaiapoi üieluedelwled : GI. I 
i 5 SIISI. IA ai : on MT 
E Nene Seen 
The figures denote the days of the month on which one or more shocks were felt. 
Those with an asterisk affixed were described as smart; those with a dagger as severe 
shocks. The remainder were only slight tremours, and no doubt escaped record at most 
om, there being no instrumental means eaplosod Le a on This table is 
th t liable so far as indicating t geographica ution of the shocks. 
